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Experimental study on the permeability characteristics of reconsolidated salt: Effects of gas and confining pressure 重固结盐渗透率特性试验研究:气相和围压的影响
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-24 DOI: 10.1016/j.ijrmms.2026.106424
Zongze Li , Jinyang Fan , Yanfei Kang , Yang Zou , Marion Fourmeau , Jie Chen , Deyi Jiang , Daniel Nelias
Reconsolidated salt, formed from crushed halite under compaction, is a promising buffer and sealing material for deep geological repositories of high-level radioactive waste (HLW) because of its low permeability and self-healing properties. This study investigated the gas permeability behavior of reconsolidated salt with varying porosities under different confining pressures and inlet gas pressures using nitrogen gas. Based on nuclear magnetic resonance (NMR) technology, the pore structure of reconsolidated salt specimens with different porosities was tested and imaged. The experimental results demonstrate that gas permeability decreases with increasing gas and confining pressures, with gas pressure having a more pronounced effect. The observed permeability‒pressure relationship is attributed primarily to the Klinkenberg effect, with gas slippage along pore walls enhancing the measured permeability under low-pressure conditions. Using the Klinkenberg correction, the absolute permeability values of reconsolidated salt were derived, reaching as low as 10−19 m2 in low-porosity samples. These values are significantly lower than the apparent gas permeability, indicating excellent sealing performance comparable to or superior to that of bentonite. A logarithmic relationship between the absolute permeability and confining pressure was established, providing a quantitative basis for permeability prediction under repository stress conditions. NMR imaging results indicate that with decreasing porosity, the connectivity between pores also gradually diminishes. Additionally, the slip factor was found to increase with increasing confining pressure, underscoring the evolving influence of pore geometry on gas transport mechanisms. Permeability of reconsolidated granular salt decreases with porosity following a power-law relationship, and the healing supports its sealing effectiveness. This study provides essential data and theoretical insights for evaluating the long-term sealing performance of reconsolidated salt in salt-based HLW repositories.
重固结盐是由岩盐压实形成的,由于其低渗透性和自愈性,是一种很有前途的高放射性废物深层地质处置库的缓冲和密封材料。利用氮气研究了不同围压和进口气体压力下不同孔隙度重固结盐的渗气行为。基于核磁共振(NMR)技术,对不同孔隙度重固结盐试样的孔隙结构进行了测试和成像。实验结果表明,渗透率随瓦斯压力和围压的增加而降低,其中瓦斯压力的影响更为明显。观察到的渗透率-压力关系主要归因于Klinkenberg效应,在低压条件下,气体沿孔壁滑动增强了测量的渗透率。利用Klinkenberg校正,导出了再固结盐的绝对渗透率值,在低孔隙度样品中渗透率可低至10 ~ 19 m2。这些值明显低于表观透气性,表明其密封性能与膨润土相当或优于膨润土。建立了绝对渗透率与围压之间的对数关系,为库区应力条件下渗透率预测提供了定量依据。核磁共振成像结果表明,随着孔隙度的减小,孔隙间的连通性也逐渐减弱。此外,滑移系数随着围压的增加而增加,这表明孔隙几何形状对气体输运机制的影响在不断变化。重固结颗粒盐的渗透率随孔隙度呈幂律关系降低,其愈合支撑了其密封效果。该研究为评价盐基高通量储存库中再固结盐的长期密封性能提供了必要的数据和理论见解。
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引用次数: 0
Microstructure-driven prediction of permeability and thermal conductivity in porous solids via a discrete multi-physics framework 基于离散多物理场框架的多孔固体渗透率和导热性的微观结构驱动预测
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-24 DOI: 10.1016/j.ijrmms.2026.106432
Changhao Liu , Andrey Jivkov , Kiprian Berbatov , Majid Sedighi , Jiangfeng Liu , Hongyang Ni
Accurate prediction of permeability and thermal conductivity of porous materials is essential for the design and optimisation of various engineering systems in energy, environmental and infrastructure applications. This study presents a discrete multi-physics modelling framework that enables direct prediction of these properties from microstructural information alone, without recourse to fitting against experimental data of fluid flow and heat transfer.
The method is based on combinatorial differential forms defined on a cell complex, allowing local conservation laws to be enforced while capturing material and interfacial non-linearities. Representative elementary volumes (REVs) were statistically reconstructed from high-resolution X-ray computed tomography (XCT) of two sandstone types, with mineralogical composition derived from X-ray diffraction (XRD) analysis. Local transport properties were assigned based on pore geometry and mineral-specific conductivities, incorporating realistic mixing rules at interfaces.
Simulations across 30 stochastic microstructural realisations per specimen of rock yielded permeability and thermal conductivity estimates that captured experimental trends and magnitudes without calibration. The results demonstrate the predictive capability and robustness of the approach, offering a viable pathway for microstructure-informed design and digital characterisation of porous and fractured geomaterials.
The central scientific contribution is a unified discrete operator formulation in which permeability and thermal conductivity emerge from the same mathematical structure, providing a physically consistent basis for modelling transport in heterogeneous and fractured rock materials.
准确预测多孔材料的渗透率和导热性对于能源、环境和基础设施应用中各种工程系统的设计和优化至关重要。本研究提出了一个离散的多物理场建模框架,可以仅从微观结构信息直接预测这些特性,而无需依赖于拟合流体流动和传热的实验数据。该方法基于在细胞复合体上定义的组合微分形式,允许在捕获材料和界面非线性的同时执行局部守恒定律。利用高分辨率x射线计算机断层扫描(XCT)对两种砂岩类型的代表性基本体积(REVs)进行了统计重建,并通过x射线衍射(XRD)分析得出了矿物成分。根据孔隙几何形状和矿物特有的导电性来分配局部输运性质,并结合界面上的实际混合规则。对每个岩石样本进行30种随机微观结构模拟,得出渗透率和导热系数估算,无需校准即可捕获实验趋势和量级。结果证明了该方法的预测能力和鲁棒性,为多孔和断裂岩土材料的微结构设计和数字化表征提供了可行的途径。其核心科学贡献是一个统一的离散算子公式,其中渗透率和导热系数来自相同的数学结构,为非均质和断裂岩石材料的运移建模提供了物理上一致的基础。
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引用次数: 0
An interpretable rock mass quality intelligent classification model (IRICM) driven by refined decision rule and its application 基于精细化决策规则驱动的可解释岩体质量智能分类模型及其应用
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-23 DOI: 10.1016/j.ijrmms.2026.106430
Xiang Wu , Fengyan Wang , Jianping Chen , Mingchang Wang , Lina Cheng , Chengyao Zhang , Junke Xu
Rock mass quality classification (RMQC) plays a crucial role in rock mass stability analysis and in the design and construction planning of rock engineering projects. However, current RMQC methods rely on expert experience, which makes it difficult for RMQC to be intelligent, scientific, and interpretable, and is not conducive to understanding rock mass characteristics in engineering applications. Therefore, this study proposes an interpretable rock mass quality intelligent classification model (IRICM) by coupling random forest (RF) and genetic algorithm (GA) to refine decision rules, aiming to enhance the intelligence, scientificity, and interpretability of RMQC. Based on 318 tunnel section data, the RMQC dataset was constructed using rock mass rating (RMR) parameters obtained from field investigations and laboratory experiments. By coupling RF and GA, the rules from all decision trees were selected, combined, and optimized to refine decision rules, achieving a classification accuracy of 87.50 % with only five rules per class. Interpretability analysis of the refined decision rules revealed that rock quality designation (RQD), intact rock strength (IRS), joint spacing (JS), and groundwater (GW) were the most frequently used features, confirming their importance in RMQC. Further analysis using post-hoc interpretability techniques also indicated that RQD, IRS, JS, and GW contributed most significantly to RMQC, especially in distinguishing poor rock mass quality (classes IV and V). The model was applied to the RMQC of tunnels and rock slopes, and the results demonstrated consistency with classification outcomes from the Q, RMR, and geological strength index (GSI) systems, validating its reliability and stability.
岩体质量分级在岩体稳定性分析和岩体工程设计与施工规划中起着至关重要的作用。然而,目前的RMQC方法依赖于专家经验,难以实现RMQC的智能化、科学性和可解释性,不利于工程应用中对岩体特征的理解。为此,本研究提出了一种可解释岩体质量智能分类模型(IRICM),通过随机森林(RF)和遗传算法(GA)的耦合来细化决策规则,以提高RMQC的智能性、科学性和可解释性。基于318条隧道断面数据,利用现场调查和室内试验获得的岩体质量等级(RMR)参数,构建RMQC数据集。通过耦合RF和GA,对所有决策树中的规则进行选择、组合和优化,以细化决策规则,实现了每类只有5条规则的分类准确率达到87.50%。精化决策规则的可解释性分析表明,岩石质量标识(RQD)、岩石完整强度(IRS)、节理间距(JS)和地下水(GW)是最常用的特征,证实了它们在RMQC中的重要性。使用事后可解释性技术的进一步分析还表明,RQD、IRS、JS和GW对RMQC的贡献最为显著,特别是在区分差岩体质量(IV类和V类)方面。将该模型应用于隧道和岩质边坡的RMQC,结果与Q、RMR和地质强度指数(GSI)系统的分类结果一致,验证了该模型的可靠性和稳定性。
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引用次数: 0
The Cosserat continuum with the hyperbolic Mohr-Coulomb failure surface and its applications to strength problems 具有双曲莫尔-库仑破坏面的Cosserat连续体及其在强度问题中的应用
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-23 DOI: 10.1016/j.ijrmms.2026.106425
Le Zhang, Hong Zheng
In the field of continuum mechanics, the Cauchy continuum model has traditionally held a dominant position. In contrast, the Cosserat continuum model, which serves as a significant complement to the Cauchy model, has primarily been used to address strain softening or to simulate the growth of shear bands. In the limited applications of the Cosserat continuum to strength problems, the elasto-plastic model employed takes the Drucker-Prager criterion as the failure criterion, rather than the Mohr-Coulomb criterion that better captures the failure characteristics of geomaterials. This is largely due to the fact that a non-smooth Mohr-Coulomb yield surface poses substantial challenges for elasto-plastic constitutive integration. To address this issue, this study develops a projection-contraction algorithm based on Gauss-Seidel iteration to implement stress updates within the framework of the Cosserat model, using a hyperbolic Mohr-Coulomb (HMC) criterion as the yield criterion. The Gauss–Seidel Projection-Contraction (GSPC) algorithm eliminates the need to compute the Hessian matrix of the yield function and exhibits superior numerical performance compared to the widely-used return-mapping method. Meanwhile, a displacement control method (DCM) is designed to bring models to the limit equilibrium state. This proposed procedure exhibits superior numerical performance compared to load control method (LCM) based on Newton iteration. Analysis of typical case studies reveals that the proposed method is free from mesh dependency and possesses robust numerical characteristics. In particular, the Cosserat continuum naturally regularizes strain localization in elastic–perfectly plastic problems, and the internal characteristic length significantly influences the thickness of shear bands and the distribution of plastic zones.
在连续介质力学领域,柯西连续介质模型历来占据主导地位。相比之下,作为柯西模型的重要补充,Cosserat连续体模型主要用于处理应变软化或模拟剪切带的生长。在Cosserat连续体对强度问题的有限应用中,所采用的弹塑性模型采用Drucker-Prager准则作为破坏准则,而不是更好地捕捉岩土材料破坏特征的Mohr-Coulomb准则。这主要是由于一个非光滑的莫尔-库仑屈服面给弹塑性本构积分带来了巨大的挑战。为了解决这一问题,本研究开发了一种基于Gauss-Seidel迭代的投影-收缩算法,以双曲Mohr-Coulomb (HMC)准则作为屈服准则,在Cosserat模型框架内实现应力更新。Gauss-Seidel投影-收缩(GSPC)算法不需要计算屈服函数的Hessian矩阵,与广泛使用的返回映射方法相比,具有优越的数值性能。同时,设计了位移控制方法(DCM),使模型达到极限平衡状态。与基于牛顿迭代的负荷控制方法(LCM)相比,该方法具有更好的数值性能。典型实例分析表明,该方法不受网格依赖,具有鲁棒性。特别是在弹塑性问题中,Cosserat连续体自然地规范了应变局部化,内部特征长度显著影响剪切带的厚度和塑性区的分布。
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引用次数: 0
Rapidly improving the acid-fracture conductivity in deep and ultra-deep carbonate reservoirs through mineral alteration: a new method 通过矿物蚀变快速提高深层和超深层碳酸盐岩储层酸缝导流能力的新方法
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-21 DOI: 10.1016/j.ijrmms.2026.106415
Xiang Chen , Zhaoxu Deng , Pingli Liu , Tianyu Zhang , Juan Du , Hongming Tang , Haitai Hu , Xuan Gao , Zhongxuan Wang , Xiaotian He
Deep and ultra-deep carbonate reservoirs contain abundant geothermal and natural gas resources, and the conductivity of acid-fractured fractures is a critical factor determining the development efficiency of these resources. However, high closure stress and acid-induced damage can lead to fracture closure and conductivity degradation. Mineral alteration refers to the in-situ conversion of existing minerals into new compounds, but the mineral alteration process is currently too slow (72 h). The Na2HPO4 + H3PO4 buffer solution (PPN) has been preliminarily proven effective in rapidly enhancing rock strength. This study investigated the effects of different acid systems (gelling acid and organic acid) and PPN treatment at 200 °C on the etching morphology, hardness, and fracture conductivity of dense carbonate rocks from two formations: the Mao-kou limestone and the Jialingjiang argillaceous limestone. The experimental results confirm that PPN rapid treatment under ultra-high temperature is effective in enhancing the fracture conductivity under high closure stress, and also reveal its mechanism of action. After 4 h of PPN treatment at 200 °C, the fracture conductivity of the Mao-kou formation and Jialingjiang formation samples increased by factors of 29.4 and 19.0, respectively, compared with untreated samples. Acid dissolution caused the rock's microstructure to transform from being dense and compact to becoming loose, with numerous dissolution pores and micro-fractures. In contrast, PPN treatment converted carbonate minerals on the fracture surfaces in situ into harder hydroxyapatite and repaired acid-induced structural damage, thereby enhancing rock strength and deformation resistance, resulting in smaller fracture-closure displacement under stress. Acid-induced damage reduced the hardness of Mao-kou formation and Jialingjiang formation samples by up to 25.6 % and 36.9 %, respectively. PPN treatment was effective for both limestone and argillaceous limestone, with the maximum increases in rock hardness reaching 39.4 % and 29.8 %, respectively. The organic acid produced a more heterogeneous etching morphology in the argillaceous limestone than the gelling acid did in the limestone. This study provides a new pathway for the rapid construction of high-conductivity fractures in deep and ultra-deep reservoir and efficient energy development.
深层和超深层碳酸盐岩储层蕴藏着丰富的地热和天然气资源,酸压裂缝的导流能力是决定这些资源开发效率的关键因素。然而,高闭合应力和酸致损伤会导致裂缝闭合和导流能力下降。矿物蚀变是指现有矿物在原位转化为新的化合物,但目前矿物蚀变过程太慢(72小时)。初步证明Na2HPO4 + H3PO4缓冲溶液(PPN)具有快速提高岩石强度的效果。研究了不同酸体系(胶凝酸和有机酸)和200℃PPN处理对茂口灰岩和嘉陵江泥质灰岩两组致密碳酸盐岩刻蚀形貌、硬度和裂缝导电性的影响。实验结果证实了超高温下PPN快速处理能有效提高高闭合应力下的裂缝导流能力,并揭示了其作用机理。经200℃PPN处理4 h后,茅口组和嘉陵江组样品的裂缝导电性分别比未处理样品提高29.4倍和19.0倍。酸溶蚀使岩石微观结构由致密致密向疏松转变,溶蚀孔和微裂缝大量存在。相比之下,PPN处理将裂缝表面的碳酸盐矿物原位转化为更硬的羟基磷灰石,修复了酸引起的结构损伤,从而提高了岩石的强度和抗变形能力,从而减小了应力作用下的缝闭位移。酸损害使茅口地层和嘉陵江地层样品的硬度分别降低25.6%和36.9%。PPN处理对灰岩和泥质灰岩均有效,岩石硬度最大增幅分别达到39.4%和29.8%。有机酸在泥质石灰岩中产生的蚀刻形态比胶凝酸在石灰岩中产生的蚀刻形态更不均匀。该研究为深层和超深层储层高导流裂缝的快速建设和高效能源开发提供了新的途径。
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引用次数: 0
Rockburst in circular openings under varying confining stress: Acoustic emission characteristics and precursors 不同围应力下圆孔岩爆:声发射特征和前兆
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-20 DOI: 10.1016/j.ijrmms.2026.106418
Yang Wang , Murat Karakus , Dongqiao Liu , Manchao He , Yunpeng Guo
Rockburst induced by high in-situ stress is a major threat to the stability of underground structures. Among various controlling factors, confining stress plays a decisive role in governing the initiation, development, and intensity of rockburst. In this study, true triaxial rockburst experiments were conducted on sandstone specimens containing a circular hole under five levels of confining stress. The failure process was monitored through real-time video and acoustic emission (AE) techniques. AE energy, entropy, and microcrack mechanisms were analyzed to characterize the evolution of failure. Two precursor indicators, namely variance based on Critical Slowing Down (CSD) theory and the Hurst exponent derived from Rescaled Range (R/S) analysis, were employed to identify early warning signals. Results show that higher confining stress leads to greater energy accumulation, stronger tangential stress concentration, more abrupt failure behavior, and increased damage brittleness. The variance parameter was more sensitive to sudden failure, whereas the Hurst exponent provided earlier indications of instability. A two-stage damage fitting model revealed accelerated damage growth and increased brittleness with rising confining stress. These findings improve the understanding of rockburst evolution under different stress conditions and contribute to the development of more reliable early warning systems for deep underground engineering.
高地应力诱发的岩爆是威胁地下结构稳定的主要因素。在各种控制因素中,围应力对岩爆的发生、发展和强度起决定性作用。本研究对含圆孔砂岩试样在5级围应力条件下进行了真三轴岩爆试验。通过实时视频和声发射(AE)技术监测破坏过程。分析了声发射能量、熵和微裂纹机制,表征了破坏的演化过程。采用两个前兆指标,即基于临界慢化(CSD)理论的方差和基于重尺度极差(R/S)分析的Hurst指数来识别预警信号。结果表明:围应力越高,能量积累越大,切向应力集中越强,破坏行为越突然,损伤脆性越高;方差参数对突然失效更敏感,而赫斯特指数提供了不稳定的早期迹象。两阶段损伤拟合模型表明,随着围应力的增加,损伤扩展加速,脆性增加。这些发现提高了对不同应力条件下岩爆演化的认识,有助于开发更可靠的深部地下工程预警系统。
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引用次数: 0
Investigation on artificial boundary problems in three-dimensional nodal-based continuous-discontinuous deformation analysis method for the seismic dynamic analyses of geotechnical structures 岩土结构地震动力分析中基于三维节点的连续-非连续变形分析方法中的人工边界问题研究
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-20 DOI: 10.1016/j.ijrmms.2026.106420
Yang Xia , Yongtao Yang , Xuhai Tang , Hong Zheng , Changfu Wei , Zuliang Shao
To accurately simulate the seismic responses of geotechnical structures using the three-dimensional nodal-based continuous-discontinuous deformation analysis method (3D-NCDDAM), appropriate boundary conditions should be set at the artificial boundaries to avoid the generation of fictitious reflected waves. In this study, various boundary conditions are used to enhance the ability of 3D-NCDDAM for seismic response analyses of geotechnical structures: (1) a viscous boundary is incorporated to absorb wave energy; (2) a viscoelastic boundary is introduced, which not only absorbs wave energy but also captures the elastic recovery behavior of the geotechnical medium; (3) based on the seismic input boundary, seismic motion is accurately applied; (4) the free field boundary applied for wave propagation in the semi-infinite domain is extended to three-dimensional space. The generation algorithm of the free field model and its coupling calculation with the main computational domain are introduced in detail; (5) the static-dynamic unified boundary introduced into 3D-NCDDAM achieves the seamless transition of boundary conditions between the quasi-static and dynamic stages. The numerical results of several examples verify the accuracy of those boundary conditions, and the entire evolution process of the landslide trigged by earthquake is effectively simulated with the enriched 3D-NCDDAM.
基于三维节点的连续-不连续变形分析方法(3D-NCDDAM)要准确模拟土工结构的地震反应,需要在人工边界处设置适当的边界条件,以避免虚拟反射波的产生。本研究采用了多种边界条件来增强3D-NCDDAM对土工结构地震反应分析的能力:(1)加入粘性边界吸收波能;(2)引入粘弹性边界,既能吸收波能,又能捕捉岩土介质的弹性恢复行为;(3)基于地震输入边界,准确应用地震运动;(4)将波在半无限域中传播的自由场边界扩展到三维空间。详细介绍了自由场模型的生成算法及其与主计算域的耦合计算;(5) 3D-NCDDAM中引入的动静统一边界实现了准静态阶段和动态阶段边界条件的无缝过渡。几个算例的数值结果验证了这些边界条件的准确性,并利用富集的3D-NCDDAM有效地模拟了地震诱发滑坡的整个演化过程。
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引用次数: 0
Mechanisms of CO2 phase transition and heat transfer in response to damage-induced permeability in coal: insights from experiment and simulation 煤损伤诱导渗透率对CO2相变和传热的响应机制:来自实验和模拟的见解
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-19 DOI: 10.1016/j.ijrmms.2026.106419
Shida Zhang , Yonggang Qiao , Nan Fan , Chaojun Fan , Danping Yuan , Xianke Wang , Yuqi Chang
Liquid carbon dioxide (LCO2) fracturing is an anhydrous technique developed to enhance coalbed methane (CBM) recovery. This study explored the influence of CO2 phase transitions on the deformation and permeability of coal subjected to LCO2 fracturing using integrated experimental observations and numerical simulations. A customized experimental setup was used to monitor temperature, pressure, coal strain, and CO2 phase transitions during distinct stages, including injection, freezing, pressure relief, and thawing. The CO2 phase exhibited dynamic evolution, transitioning sequentially from gaseous CO2 (GCO2) to liquid CO2 (LCO2), and back to GCO2. Coal was subjected to irreversible deformation driven by coupled stresses including vaporization-induced expansion, thermal stress, and freezing-induced expansion. A thermo-hydro-mechanical-damage (THMD) model accounting for variable thermophysical properties and phase transitions was established and validated experimentally. The effects of heat transfer, fluid characteristics, initial coal temperature, injection pressure, and injection temperature on CO2 phase behavior, coal damage, and permeability were systematically analyzed. The results revealed that the LCO2 freezing process involved three phases: GCO2, gas–liquid mixed CO2 (L-GCO2), and LCO2. Elevated coal temperatures intensified thermal stresses, vapor expansion forces, and freeze–thaw effects, thereby amplifying coal damage and permeability. Conversely, lower injection temperatures and higher injection pressures promoted deeper LCO2 penetration, accelerated damage progression, and significantly improved permeability. These findings offer essential theoretical insights into the optimization of the engineering performance of LCO2 fracturing technology.
液态二氧化碳(LCO2)压裂是一种用于提高煤层气采收率的无水压裂技术。本研究采用实验观测与数值模拟相结合的方法,探讨了CO2相变对LCO2压裂煤的变形和渗透率的影响。使用定制的实验装置监测不同阶段的温度、压力、煤应变和二氧化碳相变,包括注入、冻结、减压和解冻。CO2相呈现出从气态CO2 (GCO2)到液态CO2 (LCO2)再到气态CO2 (GCO2)的动态演化过程。煤在蒸发诱发膨胀、热应力和冻结诱发膨胀等耦合应力作用下发生不可逆变形。建立了考虑变热物性和相变的热-水-机械损伤(THMD)模型,并进行了实验验证。系统分析了换热、流体特性、煤的初始温度、注入压力和注入温度对CO2相行为、煤损伤和渗透率的影响。结果表明,LCO2冻结过程包括GCO2、气液混合CO2 (L-GCO2)和LCO2三个阶段。煤的温度升高加剧了热应力、蒸汽膨胀力和冻融效应,从而加剧了煤的破坏和渗透性。相反,较低的注入温度和较高的注入压力会促进LCO2渗透更深,加速损害进展,并显著提高渗透率。这些发现为优化LCO2压裂技术的工程性能提供了重要的理论见解。
{"title":"Mechanisms of CO2 phase transition and heat transfer in response to damage-induced permeability in coal: insights from experiment and simulation","authors":"Shida Zhang ,&nbsp;Yonggang Qiao ,&nbsp;Nan Fan ,&nbsp;Chaojun Fan ,&nbsp;Danping Yuan ,&nbsp;Xianke Wang ,&nbsp;Yuqi Chang","doi":"10.1016/j.ijrmms.2026.106419","DOIUrl":"10.1016/j.ijrmms.2026.106419","url":null,"abstract":"<div><div>Liquid carbon dioxide (LCO<sub>2</sub>) fracturing is an anhydrous technique developed to enhance coalbed methane (CBM) recovery. This study explored the influence of CO<sub>2</sub> phase transitions on the deformation and permeability of coal subjected to LCO<sub>2</sub> fracturing using integrated experimental observations and numerical simulations. A customized experimental setup was used to monitor temperature, pressure, coal strain, and CO<sub>2</sub> phase transitions during distinct stages, including injection, freezing, pressure relief, and thawing. The CO<sub>2</sub> phase exhibited dynamic evolution, transitioning sequentially from gaseous CO<sub>2</sub> (GCO<sub>2</sub>) to liquid CO<sub>2</sub> (LCO<sub>2</sub>), and back to GCO<sub>2</sub>. Coal was subjected to irreversible deformation driven by coupled stresses including vaporization-induced expansion, thermal stress, and freezing-induced expansion. A thermo-hydro-mechanical-damage (THMD) model accounting for variable thermophysical properties and phase transitions was established and validated experimentally. The effects of heat transfer, fluid characteristics, initial coal temperature, injection pressure, and injection temperature on CO<sub>2</sub> phase behavior, coal damage, and permeability were systematically analyzed. The results revealed that the LCO<sub>2</sub> freezing process involved three phases: GCO<sub>2</sub>, gas–liquid mixed CO<sub>2</sub> (L-GCO<sub>2</sub>), and LCO<sub>2</sub>. Elevated coal temperatures intensified thermal stresses, vapor expansion forces, and freeze–thaw effects, thereby amplifying coal damage and permeability. Conversely, lower injection temperatures and higher injection pressures promoted deeper LCO<sub>2</sub> penetration, accelerated damage progression, and significantly improved permeability. These findings offer essential theoretical insights into the optimization of the engineering performance of LCO<sub>2</sub> fracturing technology.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106419"},"PeriodicalIF":7.5,"publicationDate":"2026-01-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146000592","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Advanced thermo-hydro-mechanical modelling of Callovo-Oxfordian claystone: Temperature effects and multi-scale applications for geological disposal safety Callovo-Oxfordian粘土岩的先进热-水-力学模型:地质处置安全的温度效应和多尺度应用
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-17 DOI: 10.1016/j.ijrmms.2026.106397
M. Souley , C. De Lesquen , M.N. Vu , G. Armand
To support the feasibility of the Cigéo deep geological repository, Andra has carried out extensive thermo-hydro-mechanical (THM) investigations on Callovo-Oxfordian (COx) claystone. These investigations combine in-situ experiments conducted at the Meuse/Haute-Marne Underground Research Laboratory (M-HM URL) with detailed laboratory-scale characterisations. This study introduces an enhanced rheological model that integrates temperature-dependent mechanical characteristics derived from recent experimental data. Implemented in COMSOL Multiphysics®, the model is validated against triaxial THM tests at different temperature levels (20°, 40°, 60° and 80 °C), accurately capturing short-term strength degradation and volumetric behaviour transitions under increasing temperature. Long-term behaviour simulations, including simulation of triaxial creep tests at 40° and 60 °C, show excellent agreement with the analytical results, with deviations remaining below 0.1 %. The proposed model was first applied at the underground structures scale to the GCS drift, which serves as a reference case for validating the constitutive models of the COx claystone. The simulation covered a 20-year period, and the results were successfully compared with the convergence measurements recorded since the gallery's excavation. The model is further applied to the HITEC near-field benchmark to assess thermal impacts on the Excavation-induced Fracture Zone (EFZ) surrounding a heat-emitting waste cell. The results confirm the robustness and applicability of the proposed THM framework for large-scale repository design under thermal loading conditions.
为了支持cig深层地质储存库的可行性,Andra对Callovo-Oxfordian (COx)粘土岩进行了广泛的热-水-机械(THM)调查。这些调查结合了在默兹/上马恩地下研究实验室(M-HM URL)进行的现场实验和详细的实验室规模特征。本研究引入了一种增强的流变模型,该模型集成了来自最近实验数据的温度相关机械特性。该模型在COMSOL Multiphysics®中实现,在不同温度水平(20°、40°、60°和80°C)的三轴THM测试中进行了验证,准确捕获了温度升高下的短期强度退化和体积行为转变。长期行为模拟,包括在40°和60°C下的三轴蠕变试验模拟,与分析结果非常吻合,偏差保持在0.1%以下。该模型首次应用于地下结构尺度的GCS漂移,为验证COx粘土岩的本构模型提供了参考案例。模拟覆盖了20年的时间,结果成功地与自画廊挖掘以来记录的收敛测量结果进行了比较。该模型进一步应用于HITEC近场基准,以评估热排放废电池周围的开挖诱发裂缝带(EFZ)的热影响。研究结果验证了所提出的THM框架在热载荷条件下对大型储库设计的鲁棒性和适用性。
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引用次数: 0
Deterioration and damage characteristics of rock masses within the fluctuating zone, Three Gorges Reservoir Area, China 三峡库区波动带岩体劣化与损伤特征
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-16 DOI: 10.1016/j.ijrmms.2026.106421
Zhiqiang Yi , Yueping Yin , Zhihua Zhang , Luqi Wang , Xuebing Wang , Peng Zhao , Limei Zhang
Since 2008, the water level in the Three Gorges Reservoir Area has fluctuated annually between 145 and 175 m. This fluctuation has caused significant deterioration and damage to the rock masses within the fluctuating zone. In this zone, the elevation difference can reach up to 30 m. This study uses the Longmen dangerous rock as a typical case to comprehensively reveal the deterioration and damage characteristics of rock masses through sonic CT (Computed Tomography) imaging. This is further supported by field geological surveys, drilling engineering, and underground television. The following findings were obtained: (1) The degree of deterioration and damage below the 175 m elevation decreases with depth. Specifically, the RQD (Rock Quality Designation) generally follows an exponential distribution function. (2) The development of fractures and fragmentation zones within the fluctuating zone is higher than in areas below the fluctuating zone. (3) The degree of deterioration and damage below the 175 m elevation is heterogeneous and exhibits surface to inside pattern. (4) The essential cause of deterioration and damage effects is the RWLF (Reservoir Water Level Fluctuation). Detailed, weakly alkaline erosive flowing water in the study area initiates chemical corrosion, leading to deterioration and damage effects on the rock masses. Under the influence of gravity from the overlying high and steep dangerous rocks, leading to the prominent manifestation of joint fissures. Furthermore, mechanical dynamic effects, such as scour, erosion, and washout, occur due to the RWLF and vessels. These effects cause small portions of the rock masses to gradually detach and be carried away into the water. As a result, phenomena such as corrosion and dissolution cavities are formed. The insights gained from this study are significant for understanding the instability mechanisms of high and steep dangerous submerged rocks.
2008年以来,三峡库区水位每年在145 ~ 175 m之间波动。这种波动对波动区内的岩体造成了严重的恶化和破坏。在这个地区,高差可达30米。本研究以龙门危岩为典型案例,通过超声CT (computer Tomography)成像技术,全面揭示岩体的变质与损伤特征。现场地质调查、钻井工程和地下电视进一步支持了这一点。结果表明:(1)在海拔175 m以下,土壤劣化和破坏程度随深度的增加而减小。具体来说,RQD(岩石质量标识)通常遵循指数分布函数。(2)波动带内的裂缝破碎带发育程度高于波动带以下的区域。(3)海拔175 m以下的土壤劣化破坏程度不均匀,呈现由表向内的格局。(4)水库水位波动是水库退化和破坏的根本原因。研究区细部弱碱性侵蚀流水引发化学腐蚀,对岩体产生变质破坏作用。受上覆高陡危岩重力的影响,导致节理裂隙的突出表现。此外,由于RWLF和容器的存在,还会产生冲刷、侵蚀和冲蚀等机械动力效应。这些影响导致一小部分岩石逐渐分离并被带入水中。结果,形成了腐蚀和溶解空洞等现象。研究结果对认识高陡危险沉岩的失稳机制具有重要意义。
{"title":"Deterioration and damage characteristics of rock masses within the fluctuating zone, Three Gorges Reservoir Area, China","authors":"Zhiqiang Yi ,&nbsp;Yueping Yin ,&nbsp;Zhihua Zhang ,&nbsp;Luqi Wang ,&nbsp;Xuebing Wang ,&nbsp;Peng Zhao ,&nbsp;Limei Zhang","doi":"10.1016/j.ijrmms.2026.106421","DOIUrl":"10.1016/j.ijrmms.2026.106421","url":null,"abstract":"<div><div>Since 2008, the water level in the Three Gorges Reservoir Area has fluctuated annually between 145 and 175 m. This fluctuation has caused significant deterioration and damage to the rock masses within the fluctuating zone. In this zone, the elevation difference can reach up to 30 m. This study uses the Longmen dangerous rock as a typical case to comprehensively reveal the deterioration and damage characteristics of rock masses through sonic CT (Computed Tomography) imaging. This is further supported by field geological surveys, drilling engineering, and underground television. The following findings were obtained: (1) The degree of deterioration and damage below the 175 m elevation decreases with depth. Specifically, the RQD (Rock Quality Designation) generally follows an exponential distribution function. (2) The development of fractures and fragmentation zones within the fluctuating zone is higher than in areas below the fluctuating zone. (3) The degree of deterioration and damage below the 175 m elevation is heterogeneous and exhibits surface to inside pattern. (4) The essential cause of deterioration and damage effects is the RWLF (Reservoir Water Level Fluctuation). Detailed, weakly alkaline erosive flowing water in the study area initiates chemical corrosion, leading to deterioration and damage effects on the rock masses. Under the influence of gravity from the overlying high and steep dangerous rocks, leading to the prominent manifestation of joint fissures. Furthermore, mechanical dynamic effects, such as scour, erosion, and washout, occur due to the RWLF and vessels. These effects cause small portions of the rock masses to gradually detach and be carried away into the water. As a result, phenomena such as corrosion and dissolution cavities are formed. The insights gained from this study are significant for understanding the instability mechanisms of high and steep dangerous submerged rocks.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106421"},"PeriodicalIF":7.5,"publicationDate":"2026-01-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145980630","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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International Journal of Rock Mechanics and Mining Sciences
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